When Nature Requires a Resource to Be Used—The Case of Callinectes sapidus: Distribution, Aggregation Patterns, and Spatial Structure in Northwest Europe, the Mediterranean Sea, and Adjacent Waters
Abstract
:Simple Summary
Abstract
1. Introduction
2. Materials and Methods
2.1. Callinectes sapidus Invasion History
2.2. Distribution, Aggregation Pattern, and Spatial Structure Analyses
2.3. Callinectes sapidus Detection Methods
3. Results
3.1. Invasion History and Spatial–Temporal Patterns of Callinectes sapidus Distribution
3.2. Aggregation Patterns and Spatial Structure
- NEW—at a local spatial scale, the O–GOG* analysis showed two areas with statistically significant cold spots (99%) along the Atlantic coast of France and the Netherlands (corresponding to older records of Callinectes sapidus). The other records had non-significant index values. No hot spots and spatial outliers were detected. Medium density values were recorded in the NWE area.
- MAW—the O–GOG* analysis showed a very statistically significant cold spot (99%) in the Levantine Basin corresponding to the initial direction of spread. Hot spots (99%) were detected in the western Mediterranean Basin and eastern Atlantic Ocean. Maximum density values were recorded in the same area. Hot spots of up to 95% were also detected along the Tyrrhenian Coast of Italy and around Sicily. The occurrences in the Adriatic and Ionian Sea had non-significant index values. High spatial outliers were detected in the Levant and north Aegean Sea, and low outliers were detected in the central Mediterranean Sea.
3.3. Key Characteristics of Distribution
- NWE—from 1900, i.e., the year of the first record on the Atlantic coasts of France, to 1973, the central tendencies, measured as median and mean centres, were found in the Netherlands and Belgium, respectively. The directional dispersion of distribution and trends was concentrated along the coast, from the southwest (France) to the northeast (Denmark), with a very elongated and narrow ellipse. In the second period, i.e., 1975–1995, there is an evident contraction of the ellipse, with a strong reduction in y dispersion (from 631 to 231 km) and median and mean centres approaching each other. In the 1996–2018 period, the central tendencies diverge somewhat, and the distribution is dispersed again along the x-axis with the maximum XStdDist recorded, changing its shape but not its direction.
- MAW—from 1940, i.e., the year of the first record on the Egyptian coast, to 2000, the central tendencies, measured as median and mean centres, were found in the Aegean Sea, close to each other. The directional dispersion of distribution and trends was from southeast, in the Levantine Basin, to northwest, in the central Mediterranean Sea. In the 2001–2011 period, the central tendencies were in the southern Adriatic (Albanian coasts). The distribution’s directional dispersion changed in shape and direction, showing a considerable westward dispersion: the XStdDist ranged from 1459 km to 437 and the YStdDist from 494 km to 1552 (Table 2). This period showed the highest dispersion of Callinectes sapidus over time. This expansion is also confirmed by the distribution key characteristics in the third period (2012–2023). The ellipse is elongated from Greece to Spain, and the direction extends towards the Strait of Gibraltar. Central tendencies are shifted further west, on the western coast of Sardinia.
3.4. Callinectes sapidus Detection Methods
4. Discussion
Callinectes sapidus in the Mediterranean Sea and Adjacent Waters: A Resource to Be Used
5. Conclusions
Supplementary Materials
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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Analysis/Indicator Name | Tools | Spatial Scale | Time Scale | Ecological Meaning |
---|---|---|---|---|
Temporal and spatial–temporal pattern | ||||
Occurrence increase | Cumulative curve of occurrence | Global | All years | Occurrences increasing over time and space. Identification of invasion phases |
Occurrence increase rate | Evaluation of the slopes of the cumulative curve by the Least Squares Method | Global | NWE: 1900–1962 1963–2018 MAW: 1940–1999 2000–2010 2011–2023 | The rate of specimens increasing over time |
Density hotspots | Kernel density | Global | 1900–1949 1900–1965 1900–1986 1900–2005 1900–2015 1900–2023 | Expansion areas; nuclei of record aggregation; persistent occurrence areas; space–time occurrence density increase; highest-density areas |
Aggregation patterns and spatial structure | ||||
Global spatial autocorrelation | Global Moran’s I (GMI) NWE: cutoff distance = 350 km MAW: cutoff distance = 350 km | Global | All years | Distribution pattern: dispersion vs. random vs. clustering; change in spatial pattern over time |
Statistically significant hot spots and cold spots | Optimised hot spot analysis (O–GOG*) NWE: distance band = 95 km MAW: distance band = 200 km | Local | All years | Initial and current direction of spread and identification of dispersion/settle areas |
Spatial outliers | Anselin local Moran’s I (AMI) Cluster and outlier analysis NWE: distance band = 95 km MAW: distance band = 200 km | Local | All years | Recent records in proximity of group of older records and vice versa |
Key characteristics of distribution | ||||
Centre of gravity | Central tendency (mean centre—median centre) | Global | NWE: 1900–1973 1975–1995 1996–2018 MAW: 1940–2000 2001–2011 2012–2023 | Species concentration centre and its change over time |
Directional dispersion | XStdDist and YStdDist (km); standard deviational ellipse (1 standard deviation) | Global | Species distribution in X and Y directions | |
Directional trends | Rotation (°) Standard deviational ellipse (1 standard deviation) | Global | Directional trend in species dispersion |
Area | Years | Directional Dispersion XStdDist (km) | Directional Dispersion YStdDist (km) | Directional Trend Rotation (°) |
---|---|---|---|---|
NWE | 1900–1973 | 97 | 631 | 45 |
1975–1995 | 119 | 231 | 61 | |
1996–2018 | 175 | 558 | 59 | |
MAW | 1940–2000 | 1459 | 494 | 99 |
2001–2011 | 438 | 1553 | 86 | |
2012–2023 | 425 | 1356 | 83 |
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Castriota, L.; Falautano, M.; Perzia, P. When Nature Requires a Resource to Be Used—The Case of Callinectes sapidus: Distribution, Aggregation Patterns, and Spatial Structure in Northwest Europe, the Mediterranean Sea, and Adjacent Waters. Biology 2024, 13, 279. https://doi.org/10.3390/biology13040279
Castriota L, Falautano M, Perzia P. When Nature Requires a Resource to Be Used—The Case of Callinectes sapidus: Distribution, Aggregation Patterns, and Spatial Structure in Northwest Europe, the Mediterranean Sea, and Adjacent Waters. Biology. 2024; 13(4):279. https://doi.org/10.3390/biology13040279
Chicago/Turabian StyleCastriota, Luca, Manuela Falautano, and Patrizia Perzia. 2024. "When Nature Requires a Resource to Be Used—The Case of Callinectes sapidus: Distribution, Aggregation Patterns, and Spatial Structure in Northwest Europe, the Mediterranean Sea, and Adjacent Waters" Biology 13, no. 4: 279. https://doi.org/10.3390/biology13040279
APA StyleCastriota, L., Falautano, M., & Perzia, P. (2024). When Nature Requires a Resource to Be Used—The Case of Callinectes sapidus: Distribution, Aggregation Patterns, and Spatial Structure in Northwest Europe, the Mediterranean Sea, and Adjacent Waters. Biology, 13(4), 279. https://doi.org/10.3390/biology13040279